Schelmberge arrey is used in geoelectrical method to explore water and determine the depth of layers. In this study by using this arrey, the thickness of the layers of the studied land was determined and it was found that the first layer is not present in the northern part of the land. The difference in the depth of the next layer, which is limestone, is estimated to be about twenty meters in the northern and southern parts of the earth. This result is also consistent with the geological map of this area and shows the success of the Schlumberger arrey in predicting the fault location.